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Vegetation and climate

Vegetation–climate feedbacks modulate rainfall patterns in Africa under
future climate change

Vegetation–climate feedbacks modulate rainfall patterns in Africa under future climate change

... in vegetation structure and distribution can likewise play a role for the future regional ...regional climate model to investigate the im- pact of climatevegetation interaction for ...

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SPATIAL-TEMPORAL ANALYSES OF CLIMATE ELEMENTS, VEGETATION CHARACTERISTICS AND SEA SURFACE TEMPERATURE ANOMALY

SPATIAL-TEMPORAL ANALYSES OF CLIMATE ELEMENTS, VEGETATION CHARACTERISTICS AND SEA SURFACE TEMPERATURE ANOMALY

... Niño and La Niña events result from the tropical pacific Surface Ocean and atmospheric interaction in the ...industry and frosts. El Niño and La Niña have positive or negative influence in the ...

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Coincidences of climate extremes and anomalous vegetation responses: comparing tree ring patterns to simulated productivity

Coincidences of climate extremes and anomalous vegetation responses: comparing tree ring patterns to simulated productivity

... climatic and biospheric time series (> 50 ...data and the output from a dynamic vegetation model (LPJmL) ...productivity and offer a possibility to relate long-term tree growth to ...

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Holocene changes in African vegetation: tradeoff between climate and water availability

Holocene changes in African vegetation: tradeoff between climate and water availability

... 1998) and inhabited by humans (Kuper and Kröpelin, ...2011), and lakes and wetlands, now mostly desiccated, were widespread (Street and Grove, 1976; Hoelzmann et ...2011a). ...

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Megalake Chad impact on climate and vegetation during the late Pliocene and the mid-Holocene

Megalake Chad impact on climate and vegetation during the late Pliocene and the mid-Holocene

... variable and dependent on boundary layer ...on climate in the Chad Basin, its influence alone outside the basin is still to be deter- mined, and could be dependent on the background ...Regarding ...

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Late Holocene vegetation changes in relation with climate fluctuations and human activity in Languedoc (southern France)

Late Holocene vegetation changes in relation with climate fluctuations and human activity in Languedoc (southern France)

... Holocene climate fluctuations and human activ- ity since the Neolithic have shaped present-day Mediter- ranean ...of vegetation dynamics over the last 4500 ...historical and archeological ...

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Contribution of oceanic and vegetation feedbacks to Holocene climate change in monsoonal Asia

Contribution of oceanic and vegetation feedbacks to Holocene climate change in monsoonal Asia

... of vegetation-atmosphere and ocean-atmosphere interactions on the mid- to late Holocene climate change as well as their synergy is studied for different parts of the Asian monsoon region, giving ...

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Ecosystem Evapotranspiration as a Response to Climate and Vegetation Coverage Changes in Northwest Yunnan, China.

Ecosystem Evapotranspiration as a Response to Climate and Vegetation Coverage Changes in Northwest Yunnan, China.

... Climate and human-driven changes play an important role in regional ...China, and it has experienced severe droughts since the beginning of this century; however, the extent of the contributions from ...

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Vegetation fragment influence over urban climate

Vegetation fragment influence over urban climate

... neighborhood and to avoid natural disasters, such as erosion ...fragments and green areas in urban environment is important to an efficient management of the ...the vegetation over the urban ...

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Holocene vegetation and climate changes in central Mediterranean inferred from a high-resolution marine pollen record (Adriatic Sea)

Holocene vegetation and climate changes in central Mediterranean inferred from a high-resolution marine pollen record (Adriatic Sea)

... extent Picea around 4000 cal yr BP (Fig. 3). Increased precipitation would have in- creased river flows, bringing the poorly dispersed Abies pollen to the core location. The upper samples of the core sequence, to 3000 ...

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North African vegetation-precipitation feedback in early and mid-Holocene climate simulations with CCSM3-DGVM

North African vegetation-precipitation feedback in early and mid-Holocene climate simulations with CCSM3-DGVM

... early and middle ...orbital and greenhouse gases were not taken into ...sheet and enhanced meltwater flux into the adjacent ocean might have affected North African rainfall ...

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Asymmetry and uncertainties in biogeophysical climate–vegetation feedback over a range of CO2 forcings

Asymmetry and uncertainties in biogeophysical climate–vegetation feedback over a range of CO<sub>2</sub> forcings

... include vegetation dy- namics do not agree on the sign of precipitation anomalies in the Sahel region (Cook and Vizy, ...dependent and other ...

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Exploring the response of West Siberian wetland methane emissions to future changes in climate, vegetation, and soil microbial communities

Exploring the response of West Siberian wetland methane emissions to future changes in climate, vegetation, and soil microbial communities

... (Finlay and Clarke, 1999), due to their ease of geographic dispersal ...bogs and elsewhere suggests that differences in microbial community composition over large ge- ographic areas depend more on local ...

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Trends in Global Vegetation Activity and Climatic Drivers Indicate a Decoupled Response to Climate Change.

Trends in Global Vegetation Activity and Climatic Drivers Indicate a Decoupled Response to Climate Change.

... In a piece-wise regression, the number of segments in the PWR can vary, but for this study only two segments were used. This was done in order to restrict the influence of events with a relative short period of influence ...

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Late Holocene vegetation changes in relation with climate fluctuations and human activities in Languedoc (Southern France)

Late Holocene vegetation changes in relation with climate fluctuations and human activities in Languedoc (Southern France)

... substrates; finally, the Mountain belt is dominated by mixed forests of Abies alba and Fagus sylvatica. Pine woods are present at all altitudes, and constituted by three main different species in the study ...

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Climate-vegetation-soil interactions and long-term hydrologic partitioning: signatures of catchment co-evolution

Climate-vegetation-soil interactions and long-term hydrologic partitioning: signatures of catchment co-evolution

... geology, vegetation) and climate properties (precipitation, potential evaporation, num- ber of wet and dry days) interact at the catchment scale to produce such a simple and predictable ...

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Impacts of changes in land use and land cover on atmospheric chemistry and air quality over the 21st century

Impacts of changes in land use and land cover on atmospheric chemistry and air quality over the 21st century

... A., and Young-Molling, ...structure and function to CO 2 and climate change: results from six dynamic global vegetation models, ...

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Monitoring Growing Season Length of Deciduous Broad Leaf Forest Derived From Satellite Data in Iran

Monitoring Growing Season Length of Deciduous Broad Leaf Forest Derived From Satellite Data in Iran

... green-up and mean preseason temperature and precipitation in different preseason ...temperature and cumulative precipitation before the onset date of green-up and since preceding date of ...

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Vegetation history of Central Chukotka deduced from permafrost paleoenvironmental records of the El'gygytgyn Impact Crater

Vegetation history of Central Chukotka deduced from permafrost paleoenvironmental records of the El'gygytgyn Impact Crater

... 1979; Layer, 2000). As inferred from geomorphologic research, the study area was never glaciated after the time of the impact ca. 3.6 Myr ago (e.g. Brigham-Grette et al., 2007 and references therein). Thus, the ...

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Sub-grid scale representation of vegetation in global land surface schemes: implications for estimation of the terrestrial carbon sink

Sub-grid scale representation of vegetation in global land surface schemes: implications for estimation of the terrestrial carbon sink

... McGuire, A. D., Sitch, S., Clein, J. S., Dargaville, R., Esser, G., Foley, J., Heimann, M., Joos, F., Kaplan, J., Kicklighter, D. W., Meier, R. A., Melillo, J. M., Moore, B., Prentice, I. C., Ra- mankutty, N., Reichenau, ...

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